Spatio-Temporal Modelling of Lightning Climatologies for Complex Terrain
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Age and Structure of the Stolzalpe Nappe
AgeAge andand structurestructure ofof thethe StolzalpeStolzalpe nappenappe -- EvidenceEvidence forfor VariscanVariscan metamorphism,metamorphism, EoalpineEoalpine top-to-the-WNWtop-to-the-WNW thrustingthrusting andand top-to-the-ESEtop-to-the-ESE normalnormal faultingfaulting (Gurktal(Gurktal Alps,Alps, Austria)Austria) Geological Survey of Austria C. IGLSEDER1,*) , B. HUET1,*) , G. RANTITSCH2,*), L. RATSCHBACHER3,*) & J. PFÄNDER3,*) INTRODUCTION: OVERVIEW: 17° 16° 15° 14° 10° 11° 12° 13° Tectonic map of the Alps Passau S.M. Schmid, B. Fügenschuh, E. Kissling and R. Schuster , 2004 Donau Inn In the Gurktal Alps (Austria,) the Drauzug-Gurktal nappe system represents the Graphics : S. Lauer Wien 5° 6° 48° 48° 7° München 8° 9° 5240000 Rhein Basel Zürich uppermost tectonic part of the Upper Austro-Alpine nappe stack. The Stolzalpe Nappe Besancon 47° 47° Graz Bern Maribor ± Drava (s. str.) is its uppermost unit. It consists of interbedded metasedimentary rocks of the Genève 46° 46° Rhone T Zagreb agliamento Sava 5230000 Trieste Milano Venezia Verona Padova Spielriegel Complex, overlain by metavolcanic rocks of the Kaser-Eisenhut Complex. Grenoble Torino 45° 45° Po 17° Po 16° 15° 14° 100 km 11° 12° 13° Both are covered by the Pennsylvanian clastic Stangnock Formation. In the Genova 44° Durance 5° 6° Nice 7° 8° 9° 10° investigated area, located at UTM-map sheet Radenthein (NL-33-04-06), the 5220000 Stolzalpe Nappe tectonically overlays the Stangnock Formation belonging to the Tectonic map of the investigated area Königstuhl Subnappe, also part -
AUSTRIAN JOURNAL of EARTH SCIENCES Volume 98 2005
© Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at AUSTRIAN JOURNAL of EARTH SCIENCES [MITTEILUNGEN der ÖSTERREICHISCHEN GEOLOGISCHEN GESELLSCHAFT] an INTERNATIONAL JOURNAL of the AUSTRIAN GEOLOGICAL SOCIETY volume 98 2005 István DUNKL, Joachim KUHLEMANN, John REINECKER & Wolfgang FRISCH: Cenozoic relief evolution of the Eastern Alps – constraints from apatite fission track age-provenance of Neogene intramontane sediments__________________________________________________________________________ www.univie.ac.at/ajes EDITING: Grasemann Bernhard, Wagreich Michael PUBLISCHER: Österreichische Geologische Gesellschaft Rasumofskygasse 23, A-1031 Wien TYPESETTER: Irnberger Norbert, www.irnberger.net Copy-Shop Urban, Bahnstraße 26a, 2130 Mistelbach PRINTER: Holzhausen Druck & Medien GmbH Holzhausenplatz 1, 1140 Wien ISSN 0251-7493 © Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Austrian Journal of Earth Sciences Volume 98 Vienna 2005 Cenozoic relief evolution of the Eastern Alps – con- straints from apatite fission track age-provenance of Neogene intramontane sediments István DUNKL1)*), Joachim KUHLEMANN2), John REINECKER2) & Wolfgang FRISCH2) KEYWORDS paleogeography fission track provenance 1) Sedimentology, Geoscience Center, University of Göttingen exhumation 2) Institute of Geosciences, University of Tübingen sediment relief *) Corresponding author, [email protected] Alps Abstract Fission track (FT) ages -
TAUERN SPA Zell Am See – Kaprun PRESS KIT 2020
Kaprun 2020 TAUERN SPA Zell am See – Kaprun PRESS KIT 2020 Kaprun 2020 Content: Expedition New Heights Wellness Family Culinary Relax! Day SPA Seminars, Meetings & Events All abot the TAUERN SPA Golf Getting out into nature Everything at a glance Kaprun 2020 Press information: New Heights Expedition TAUERN SPA Zell am See – Kaprun Expedition New Heights. The exclusive 4*S resort at the foot of the Kitzsteinhorn is growing with the region and has extended its facilities and services since autumn 2019. With additional 52 nature & garden rooms, a spectacular new glass panorama pool and many other innovative highlights, the 4*S resort provides its guests an unparalleled and unforgettable holiday. For all who want to scale new heights. The popular TAUERN SPA extended its offer in November 2019 and delights it´s guest with ambitious innovations and service upgrades right across the hotel, SPA, rooms and culinary services. The existing accommodation has been extended northwards and north-eastwards and includes 52 new garden & nature rooms on four levels. The architecture of the extension, with its organic shape and green roof, blends harmoniously into the landscape. Turning dreams (and rooms) into reality The new garden & nature rooms mainly use natural materials such as swiss stone pine, sandstone, leather and wool to create a unique, and cosy ambiance. The philosophy here is all about green & clean living: High-quality sleeping systems, a healthness bath and the most modern technical equipment are part of the complete equipment of every room. Digital detox at it´s best: a button, that can be used to deactivate disturbing power sources around the head area, helps you to get deep and healthy sleep. -
Lichenotheca Graecensis, Fasc
- 1 - Lichenotheca Graecensis, Fasc. 23 (Nos 441–480) Walter OBERMAYER* OBERMAYER Walter 2017: Lichenotheca Graecensis, Fasc. 23 (Nos 441– 480). - Fritschiana (Graz) 87: 1–13. - ISSN 1024-0306. Abstract: Fascicle 23 of 'Lichenotheca Graecensis' comprises 40 collections of lichens from the following countries (and ad- ministrative subdivisions): Albania, Australia (New South Wales; Norfolk Island; Queensland; Western Australia), Austria (Carin- thia; Salzburg; Styria; Upper Austria), Germany (Baden-Würt- temberg), Greece (Corfu Island), Spain (Mallorca), Switzerland (Canton of Jura), and U.S.A. (Alaska). Isotypes of Caloplaca dahlii, C. norfolkensis, and Trapeliopsis granulosa var. australis are distributed. TLC-analyses were carried out for Chrysothrix candelaris, Cladonia rei, Hypogymnia physodes (growing on ground), Hypotrachyna revoluta aggregate, Lepra albescens, Le- praria caesioalba, L. crassissima aggregate, Melanohalea exas- perata, Parmotrema arnoldii, Parmotrema reticulatum aggregate, Pycnora sorophora, Ramalina capitata, R. fraxinea, and Trapeli- opsis pseudogranulosa. *Institut für Pflanzenwissenschaften, NAWI Graz, Karl-Franzens- Universität, Holteigasse 6, 8010 Graz, AUSTRIA e-mail: [email protected] Introduction The exsiccata series 'Lichenotheca Graecensis' is distributed on exchange basis to the following 19 public herbaria and to one private collection (herbarium ab- breviations follow http://sweetgum.nybg.org/science/ih/): ASU, B, C, CANB, CANL, E, G, GZU, H, HAL, HMAS, LE, M, MAF, MIN, O, PRA, TNS, UPS, Klaus KALB. A pdf- file of the exsiccata is stored under https://static.uni-graz.at/fileadmin/ nawi- institute/Botanik/Fritschiana/fritschiana-87/lichenotheca-graecensis-23.pdf. A text version can be found under https://homepage.uni-graz.at/de/walter.obermayer/ publications/lichenotheca-graecensis-textfile-of-all-issues/. Label texts originally drafted in a local language have been translated into English by the author. -
Dwelling Lichens After Glacier Retreat in the European Alps
Journal of Biogeography (J. Biogeogr.) (2017) ORIGINAL Assembly patterns of soil-dwelling ARTICLE lichens after glacier retreat in the European Alps Juri Nascimbene1* , Helmut Mayrhofer2, Matteo Dainese3 and Peter Othmar Bilovitz2 1Department of Biological, Geological and ABSTRACT Environmental Sciences, University of Aim To assess the spatial-temporal dynamics of primary succession following Bologna, I-40126 Bologna, Italy, 2Institute of deglaciation in soil-dwelling lichen communities. Plant Sciences, NAWI Graz, University of 3 Graz, 8010 Graz, Austria, Department of Location European Alps (Austria, Switzerland and Italy). Animal Ecology and Tropical Biology, Biocenter, University of Wurzburg,€ 97074 Methods Five glacier forelands subjected to relevant glacier retreat during the Wurzburg,€ Germany last century were investigated. In each glacier foreland, three successional stages were selected at increasing distance from the glacier, corresponding to a gradi- ent of time since deglaciation between 25 and 160 years. In each successional stage, soil-dwelling lichens were surveyed within five 1 9 1 m plots. In addi- tion to a classical ecological framework, based on species richness and compo- sition, we applied a functional approach to better elucidate community assembly mechanisms. Results A positive relationship was found between species richness and time since deglaciation indicating that richer lichen communities can be found at increasing terrain ageing. This pattern was associated with compositional shifts, suggesting that different community assemblages can be found along the suc- cessional stages. The analysis of b-diversity revealed a significant nested pattern of species assemblages along the gradient (i.e. earlier successional stages hosted a subset of the species already established in older successional stages), while the turnover component was less relevant. -
17 Small Historic Towns in Austria
17 SMALL 2021/2022 HISTORIC TOWNS IN AUSTRIA SEE EXPERIENCE ENJOY SMALL HISTORIC TOWNS www.khs.info SMALL HISTORIC TOWNS WHAT MAKES US STAND OUT: Well-preserved historic townscapes Heritage buildings and landmarks Spectacular surrounding landscapes Scheduled tours with qualified guides Varied, high-quality events and shows Traditional weekly markets Traditional crafts in that you can experience first-hand Tourist attractions and experiences Lively cultural programmes Refined cuisine Unique shopping Medieval town charters Populations of less than 45,000 SMALL HISTORIC TOWNS IN AUSTRIA Stadtplatz 27 | 4402 Steyr | Austria Tel. +43 72 52 522 90 [email protected] | www.khs.info EXPLORE EACH TOWN IN 48 HOURS ... SEE EXPERIENCE ENJOY EDITORIAL / MAP 4 – 5 1 BADEN bei WIEN The furnished garden 6 – 13 2 BAD ISCHL Tradition and modernity 14 – 21 3 BAD RADKERSBURG Walking and cycling 22 – 29 4 BLUDENZ A wealth of possibilities 30 – 37 5 BRAUNAU am INN Charm and comfort on the Inn river 38 – 45 6 BRUCK a. d. MUR Nature and culture combined 46 – 53 7 FREISTADT A Varied History 54 – 61 8 GMUNDEN A stylish town of leisure 62 – 69 9 HALLEIN A multifacted insider tip 70 – 77 10 HARTBERG The garden town 78 – 85 11 JUDENBURG Flying high 86 – 93 12 KUFSTEIN Cobblestones meet modern urban flair 94 – 101 13 LEOBEN Attractive town with great views 102 – 109 14 RADSTADT A break with a view 110 – 117 15 SCHÄRDING Baroque treasure trove 118 – 125 16 STEYR When culture’s your fancy 126 – 133 17 WOLFSBERG Castles, mountains and wolves 134 – 141 AUSTRIA CLASSIC TOUR 142 – 143 3 Markus Deisenberger, freelance journalist; lives and works in Salzburg and Vienna Dear travellers, connoisseurs and friends of the SMALL HISTORIC TOWNS of Austria, A5 It typically takes about two days for visitors and tourists to Freistadt Wien get to know a town. -
NATIONALISM TODAY: CARINTHIA's SLOVENES Part I: the Legacy Ofhistory by Dennison I
SOUTHEAST EUROPE SERIES Vol. XXII No. 4 (Austria) NATIONALISM TODAY: CARINTHIA'S SLOVENES Part I: The Legacy ofHistory by Dennison I. Rusinow October 1977 The bombsmostly destroying Osvobodilna other world is Slovene, and in the valleys of Carin- Fronta or AbwehrMimpfer monumentshave been thia, the two peoples and cultures have been mixed too small and too few and have done too little for more than eleven hundred years. Until the damage to earn much international attention in this "national awakening" of the nineteenth century, age of ubiquitous terrorism in the name of some nobody seems to have minded. Then came the Slo- ideological principle or violated rights. Moreover, vene renaissance and claims to cultural and social the size of the national minority in question, the equality for Slovenes qua Slovenes, backed by the quality of their plight, and the potentially wider shadows of Austro-Slavism, South-(Yugo-)Slavism, Austrian and international repercussions ofthe con- and pan-Slavism. The German Carinthians, feeling flict all pale into insignificance alongside the prob- threatened in their thousand-year cultural, political, lems of the Cypriots, of the Northern Irish, of the and economic dominance on the borderland, Basques, of the Palestinian and Overseas Chinese reacted with a passion that became obsessive and diasporas, of the non-Russian peoples of the Soviet that was to culminate in Nazi attempts during Union, or of many others. Despite these disclaimers, World War II to eradicate the Slovene Carinthians however, the problem of the Carinthian Slovenes is through a combination of forcible assimilation and worth examining for more than its local and population transfers. -
Late Miocene Increasing Exhumation Rates in the Eastern Part of the Alps – Implications from Low Temperature Thermochronology
doi: 10.1111/ter.12221 Late Miocene increasing exhumation rates in the eastern part of the Alps – implications from low temperature thermochronology Andreas W€olfler,1 Walter Kurz,2 Harald Fritz,2 Christoph Glotzbach1 and Martin Danisık3 1Institut fur€ Geologie, Leibniz Universitat€ Hannover, Callinstraße 30, Hannover D-30167, Germany; 2Institut fur€ Erdwissenschaften, Karl-Franzens Universitat€ Graz, Graz A-8010, Austria; 3John de Laeter Centre for Isotope Research, Department of Applied Geology, The Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA 6845, Australia ABSTRACT A new set of apatite fission-track and apatite (U–Th)/He data operated simultaneously during lateral extrusion of the East- reveals a hitherto undated late Miocene exhumation pulse in ern Alps. As the higher late Miocene/Pliocene exhumation the eastern part of the Eastern Alps. While distinct parts of rates are restricted to a single tectonic block, namely the Nie- the study area, including the Seckauer Tauern, have been at dere Tauern, we infer a tectonic trigger that is probably near surface conditions (<100 °C) since the Eocene, the neigh- related to a change in the external stress field that affected bouring Niedere Tauern experienced enhanced cooling and the Alps during this time. exhumation in the middle Miocene and again at the late Mio- cene/Pliocene boundary. Middle Miocene exhumation is inter- Terra Nova, 00: 1–9, 2016 preted as a result of tectonic escape and convergence that thermochronological point of view, and perturbation of isotherms, which Introduction this part of the Alps is less well may result in false conclusions about The existing low-temperature ther- investigated than other areas such as exhumation rates in the upper crust mochronological datasets from the the Tauern Window or the Western (Stuwe€ et al., 1994; Braun, 2002). -
Nota Lepidopterologica
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Nota lepidopterologica Jahr/Year: 2010 Band/Volume: 33 Autor(en)/Author(s): Cupedo Frans Artikel/Article: A revision of the infraspecific structure of Erebia euryale (Esper, 1805) (Nymphalidae: Satyrinae) 85-106 ©Societas Europaea Lepidopterologica; download unter http://www.biodiversitylibrary.org/ und www.zobodat.at Nota lepid.33 (1): 85-106 85 A revision of the infraspecific structure of Erebia euryale (Esper, 1805) (Nymphalidae: Satyrinae) Frans Cupedo Processieweg 2, NL-6243 BB Geulle, Netherlands; [email protected] Abstract. A systematic analysis of the geographic variation of both valve shape and wing pattern reveals that the subspecies ofErebia euryale can be clustered into three groups, characterised by their valve shape. The adyte-group comprises the Alpine ssp. adyte and the Apenninian brutiorum, the euryale-group in- cludes the Alpine subspecies isarica and ocellaris, and all remaining extra- Alpine occurrences. The third group (kunz/-group), not recognised hitherto, is confined to a restricted, entirely Italian, part of the south- ern Alps. It comprises two subspecies: ssp. pseudoadyte (ssp. n.), hardly distinguishable from ssp. adyte by its wing pattern, and ssp. kunzi, strongly melanistic and even exceeding ssp. ocellaris in this respect. The ssp. pseudoadyte territory is surrounded by the valleys of the rivers Adda, Rio Trafoi and Adige, and ssp. kunzi inhabits the eastern Venetian pre-Alps, the Feltre Alps and the Pale di San Martino. The interven- ing region (the western Venetian pre-Alps, the Cima d'Asta group and the Lagorai chain) is inhabited by intermediate populations. -
Holidays of All Kinds in Carinthia – the Ski Season on the Mölltal Glacier Begins and So Does the Hiking Season in Ankogel
Holidays of all kinds in Carinthia – the ski season on the Mölltal glacier begins and so does the hiking season in Ankogel Flattach – 19th May – Tourism in Austria is slowly getting off the ground. After pandemic restrictions were loosened on 19th May, life is returning to the ski resorts and tourist centres in Carinthia too. Top conditions attract skiers to come to Mölltaler Gletscher, tourists to hike in the beautiful Ankogel resort and cyclists to zip through magical valleys at the foot of the High Tauern. Mölltaler Gletscher – the only glacier in Carinthia is reopening on 22nd May 2021. Recreational skiers and sport clubs can enjoy more than 3 metres of snow on the pistes. “The Schareck 1, 2, 3 pistes will be available for skiers and so will be the almost 3- kilometre-long red Eissee piste no. 9, which runs to the lower cable car station and is usually not at disposal at this time of the year. Our resort will be opened also for tourists, of course, and is ready to serve as a popular starting point or outlook spot. After the restrictions have been loosened, hotels and guest houses could reopen and simpler rules of border crossing for vaccinated people have been announced, we expect that our glacier will welcome recreation seekers as well as training athletes,” said Max Gottfried, the resort general manager. Tourists and skiers coming to the Mölltaler Gletscher resort can travel with the Mölltaler Gletscher Express funicular, the Gondelbahn Eissee cable car, the Gletscher Jet 6-seater chairlift or the 3000er chairlift depending on the conditions. -
THE 5***** GRAND HOTEL LIENZ .Indd
AUSTRIA Clip Lienz The unknown Pearl of the Dolomites Your upcoming unique holiday experience Lienz is located in the heart of the Alps at the confluence of the rivers Isel and Drava, close to the highest Austrian mountain Grossglockner. After a three hour scenic ride you reach your unique mountain refuge from the International Airports in Venice or Munic by private transfer. Due to its perfect location and its sustainable tourism development over the past decades, Lienz still offers a full intact, vibrant and authentic local life which combines traditions and modernity alike. You will be fascinated by the natural beauty with ever cooling glacier rivers, beautiful shaped mountain lakes, waterfalls and gorgeous mountain formations in the midst of the highest mountains of the Eastern Alps. Lienz – certainly a place of highest quality of life! Lienz is loved by locals and holidaymakers likewise. Especially in summer, the beautiful town stands out by its unique flair. Here, life can still be enjoyed to the fullest, far away from rumbling cities, pollution, heat and dust, Lienz will welcome you with a light breeze of fresh mountain air, with cool water from glacier rivers, significant rainfalls, stunning mountain lakes and adorable Alpine meadows and forests! Enjoy and relax in an unique environment, regain strength, let your soul dangle and renew your energies! THE 5***** GRAND HOTEL LIENZ This luxury 5-star hotel offers an exclusive ambiance in the heart of the picturesque town of Lienz in East Tyrol, surrounded by the scenic mountains of the Lienz Dolomites. Guests benefit from a large spa area and a gourmet restaurant. -
Benedek-Et-Al-2001.Pdf
Int J Earth Sciences Geol Rundsch) 2001) 90 : 519±533 DOI 10.1007/s005310000183 ORIGINAL PAPER K. Benedek ´ Z.R. Nagy ´ I. Dunkl ´ C. Szabó S. Józsa Petrographical, geochemical and geochronological constraints on igneous clasts and sediments hosted in the Oligo-Miocene Bakony Molasse, Hungary: evidence for a Paleo-Drava River system Received: 20 April 2000 / Accepted: 15 November 2000 / Published online: 17 March 2001 Springer-Verlag 2001 Abstract The provenance of igneous clasts and aren- FT age mean: ~34.7 Ma) were derived from the Peri- itic sediment enclosed within the Bakony Molasse was adriatic intrusives and their contact zones.On the studied using geochemical and geochronological meth- basis of the new data, we propose that the ancestor of ods.The majority of igneous clasts were eroded from the recent Drava River had already existed in Oligo- the Oligocene Periadriatic magmatic belt.A part of Miocene time and distributed eroded material of the the andesite material has Eocene formation age. southern Eastern Alps to the east. Rhyolitic pebbles originated from Permian sequences of the Greywacke zone or the Gurktal Alps.Apatite Keywords Alpine Molasse ´ Fission track dating ´ fission track FT) ages from the sandstone matrix age K/Ar dating ´ Geochemistry ´ Provenance analysis ´ clusters at ~75 and ~30 Ma) are typical for the Aus- Pannonian Basin ´ Oligocene±Miocene troalpine nappe pile and for the cooling ages of Peri- adriatic magmatic belt.Variscan detrital zircon FT ages indicate source areas that had not suffered Introduction Alpine metamorphism, such as the Bakony Mountains, Drauzug and the Southern Alps.Another group of The Alpine collision and subsequent uplift resulted in detrital zircon grains of Late Triassic±Jurassic FT age the formation of numerous alluvial systems during Oli- mean: ~183 Ma) marks source zones with Mesozoic go-Miocene time in the Alpine±Carpathian region.